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Trata-se de um conjunto de informações gráficas (pontos, linhas e polÃgonos) e alfanuméricas, georreferenciadas, interpretadasem escala 1:250.000, que retratam caracterÃsticas geomorfológicas da Folha XXX conforme metodologia contida no Manual Técnicode Geomorfologia (ftp://geoftp.ibge.gov.br/documentos/recursos_naturais/manuais_tecnicos/manual_tecnico_geomorfologia.pdf). São delineados e descritos polÃgonos de modelados de relevo contendo suanatureza genética, Unidade e Região Geomorfológica e o DomÃnio Morfoestrutural no qual estão inseridos. Também são representadas,por linhas e pontos, as principais formas de relevo encontradas no paÃs.A metodologia descrita no Manual Técnico de Geomorfologia é uma evolução dos procedimentos metodológicos adotados pelo projetoRADAMBRASIL no mapeamento geomorfológico do Brasil na escala de 1:1.000.000. O processo de elaboração dos mapas consistedas seguintes etapas: (1) estudo preliminar da área com a aquisição de bibliografia, documentos cartográficos e produtosde sensoreamento remoto, (2) elaboração de mapa geomorfológico preliminar com a análise da drenagem e delimitação de modeladose formas de relevo, apontando os locais de dúvida e de interesse para a terceira etapa, (3) atividade de campo, que tem comoobjetivo, além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campoe registros fotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamentodas informações gráficas e alfanuméricas em banco de dados para posterior consulta, tratamento,e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSE21.fid-6d9cbe3e_18e3b294723_66ce |
Folha |
SE21 |
Legenda_Completa |
496Dc43 |
Nome_Dominio |
Bacias e Coberturas Sedimentares Fanerozóicas |
Nome_Regiao |
Planaltos e Patamares da Borda Ocidental da Bacia do Paraná |
Identificacao_Unidade |
496 |
Nome_Unidade |
Segundo Patamar da Borda Ocidental da Bacia do Paraná |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
médio : > 100 a 150m |
Nivel_Altimetrico |
|
Legenda |
Segundo Patamar da Borda Ocidental da Bacia do Paraná |
Area_Poligono_Km2 |
25.518 |
the_geom |
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gov
Trata-se de um conjunto de informações gráficas (pontos, linhas e polÃgonos) e alfanuméricas, georreferenciadas, interpretadasem escala 1:250.000, que retratam caracterÃsticas geomorfológicas da Folha XXX conforme metodologia contida no Manual Técnicode Geomorfologia (ftp://geoftp.ibge.gov.br/documentos/recursos_naturais/manuais_tecnicos/manual_tecnico_geomorfologia.pdf). São delineados e descritos polÃgonos de modelados de relevo contendo suanatureza genética, Unidade e Região Geomorfológica e o DomÃnio Morfoestrutural no qual estão inseridos. Também são representadas,por linhas e pontos, as principais formas de relevo encontradas no paÃs.A metodologia descrita no Manual Técnico de Geomorfologia é uma evolução dos procedimentos metodológicos adotados pelo projetoRADAMBRASIL no mapeamento geomorfológico do Brasil na escala de 1:1.000.000. O processo de elaboração dos mapas consistedas seguintes etapas: (1) estudo preliminar da área com a aquisição de bibliografia, documentos cartográficos e produtosde sensoreamento remoto, (2) elaboração de mapa geomorfológico preliminar com a análise da drenagem e delimitação de modeladose formas de relevo, apontando os locais de dúvida e de interesse para a terceira etapa, (3) atividade de campo, que tem comoobjetivo, além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campoe registros fotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamentodas informações gráficas e alfanuméricas em banco de dados para posterior consulta, tratamento,e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSE21.fid-6d9cbe3e_18e3b294723_66cf |
Folha |
SE21 |
Legenda_Completa |
484Dc41 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planalto da Bodoquena |
Identificacao_Unidade |
484 |
Nome_Unidade |
Serra da Bodoquena |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Serra da Bodoquena |
Area_Poligono_Km2 |
0.727 |
the_geom |
MULTIPOLYGON (((-57.03558343528486 -19.89190722667725, -57.03441060601851 -19.892252289941318, -57.03393091254948 -19.89363293722713, -57.03406002703301 -19.8952391096506, -57.03407329761213 -19.89770768321473, -57.033893952436316 -19.898396503504873, -57.03239153493022 -19.90138965068427, -57.03221343763009 -19.90202098798048, -57.03221663115789 -19.902710658743974, -57.03246285890511 -19.903397868066172, -57.0330711914192 -19.903911676318863, -57.03374129946238 -19.904367382215646, -57.0345918568233 -19.904477302028884, -57.035502559963156 -19.904471658283907, -57.03671107497962 -19.903720298715186, -57.03725687407244 -19.903316024142665, -57.03773859335628 -19.902854026001986, -57.0389482445852 -19.901870951579237, -57.03943122189672 -19.90135236235303, -57.03991248562306 -19.90060389014368, -57.040212256236124 -19.900027891035034, -57.04026733628116 -19.898650628728518, -57.040202654300195 -19.89796248710447, -57.03995574326425 -19.897217825106004, -57.03958941820927 -19.896530953562763, -57.038430327522335 -19.895331271306834, -57.03788223829756 -19.894875245137193, -57.037393918455244 -19.894188715100427, -57.03684382088004 -19.89355938835595, -57.03653744897172 -19.892987756731603, -57.03558343528486 -19.89190722667725))) |
gov
Trata-se de um conjunto de informações gráficas (pontos, linhas e polÃgonos) e alfanuméricas, georreferenciadas, interpretadasem escala 1:250.000, que retratam caracterÃsticas geomorfológicas da Folha XXX conforme metodologia contida no Manual Técnicode Geomorfologia (ftp://geoftp.ibge.gov.br/documentos/recursos_naturais/manuais_tecnicos/manual_tecnico_geomorfologia.pdf). São delineados e descritos polÃgonos de modelados de relevo contendo suanatureza genética, Unidade e Região Geomorfológica e o DomÃnio Morfoestrutural no qual estão inseridos. Também são representadas,por linhas e pontos, as principais formas de relevo encontradas no paÃs.A metodologia descrita no Manual Técnico de Geomorfologia é uma evolução dos procedimentos metodológicos adotados pelo projetoRADAMBRASIL no mapeamento geomorfológico do Brasil na escala de 1:1.000.000. O processo de elaboração dos mapas consistedas seguintes etapas: (1) estudo preliminar da área com a aquisição de bibliografia, documentos cartográficos e produtosde sensoreamento remoto, (2) elaboração de mapa geomorfológico preliminar com a análise da drenagem e delimitação de modeladose formas de relevo, apontando os locais de dúvida e de interesse para a terceira etapa, (3) atividade de campo, que tem comoobjetivo, além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campoe registros fotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamentodas informações gráficas e alfanuméricas em banco de dados para posterior consulta, tratamento,e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSE21.fid-6d9cbe3e_18e3b294723_66d0 |
Folha |
SE21 |
Legenda_Completa |
484Da51 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planalto da Bodoquena |
Identificacao_Unidade |
484 |
Nome_Unidade |
Serra da Bodoquena |
Letra_Simbolo |
Da |
Categoria |
Homogênea aguçada |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo aguçado |
Densidade_Drenagem |
muito alta |
Aprofundamento_Incisoes |
muito fraco : até 50m |
Nivel_Altimetrico |
|
Legenda |
Serra da Bodoquena |
Area_Poligono_Km2 |
2.164 |
the_geom |
MULTIPOLYGON (((-56.80157434122532 -20.000558777301993, -56.80178849023255 -19.99808016393766, -56.80182169290637 -19.99642528689372, -56.80207464535174 -19.995277661072336, -56.80210946327385 -19.991083472407045, -56.80223663115221 -19.9903951354722, -56.80248655563414 -19.989593371697296, -56.803223476272905 -19.988679261390722, -56.803349679120856 -19.987990936911938, -56.803728065433646 -19.986443347174504, -56.80373715019257 -19.9854085122541, -56.803388474845974 -19.98345276669445, -56.80321523101203 -19.9825319234652, -56.802258458911396 -19.98068517874534, -56.801776911695626 -19.980049264290933, -56.80179310995895 -19.978153000368724, -56.80174097614219 -19.977233728799796, -56.8006465919241 -19.97734007885479, -56.79985286282895 -19.977793013337827, -56.79942069793193 -19.978537175581252, -56.79887142424103 -19.978934828048455, -56.79843855362925 -19.9797930697288, -56.79824786585302 -19.980652641216704, -56.797689121940046 -19.982141708243798, -56.79750071694812 -19.98294557340834, -56.79743271319388 -19.983865082705634, -56.79724131757112 -19.984838742056525, -56.79717400440655 -19.98564327684418, -56.79674277022648 -19.986386541963977, -56.79667413848822 -19.987247679936978, -56.79624359265049 -19.987875967979125, -56.796176968074505 -19.988565528965623, -56.79574615057019 -19.989078847718513, -56.79531621401166 -19.98976461802125, -56.794824151158245 -19.990392583995913, -56.79323417230047 -19.99170177719647, -56.79219417638396 -19.99249743495021, -56.79096643576558 -19.993981992080627, -56.79016715070562 -19.995181406418467, -56.78973728104231 -19.995695613781603, -56.78899182646943 -19.997527789998056, -56.78880338365095 -19.998331679055184, -56.78854030012336 -19.99916590710671, -56.78850468776495 -19.99997196819489, -56.78866998123426 -20.000561525691896, -56.79198919788197 -20.000561458260353, -56.792128431514875 -20.000561454627455, -56.79252728928431 -20.00056144386152, -56.79970358078924 -20.000559078319046, -56.801559405896576 -20.00055878030636, -56.80157434122532 -20.000558777301993))) |
gov
Trata-se de um conjunto de informações gráficas (pontos, linhas e polÃgonos) e alfanuméricas, georreferenciadas, interpretadasem escala 1:250.000, que retratam caracterÃsticas geomorfológicas da Folha XXX conforme metodologia contida no Manual Técnicode Geomorfologia (ftp://geoftp.ibge.gov.br/documentos/recursos_naturais/manuais_tecnicos/manual_tecnico_geomorfologia.pdf). São delineados e descritos polÃgonos de modelados de relevo contendo suanatureza genética, Unidade e Região Geomorfológica e o DomÃnio Morfoestrutural no qual estão inseridos. Também são representadas,por linhas e pontos, as principais formas de relevo encontradas no paÃs.A metodologia descrita no Manual Técnico de Geomorfologia é uma evolução dos procedimentos metodológicos adotados pelo projetoRADAMBRASIL no mapeamento geomorfológico do Brasil na escala de 1:1.000.000. O processo de elaboração dos mapas consistedas seguintes etapas: (1) estudo preliminar da área com a aquisição de bibliografia, documentos cartográficos e produtosde sensoreamento remoto, (2) elaboração de mapa geomorfológico preliminar com a análise da drenagem e delimitação de modeladose formas de relevo, apontando os locais de dúvida e de interesse para a terceira etapa, (3) atividade de campo, que tem comoobjetivo, além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campoe registros fotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamentodas informações gráficas e alfanuméricas em banco de dados para posterior consulta, tratamento,e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSE21.fid-6d9cbe3e_18e3b294723_66d1 |
Folha |
SE21 |
Legenda_Completa |
484Dc42 |
Nome_Dominio |
Cinturões Móveis Neoproterozóicos |
Nome_Regiao |
Planalto da Bodoquena |
Identificacao_Unidade |
484 |
Nome_Unidade |
Serra da Bodoquena |
Letra_Simbolo |
Dc |
Categoria |
Homogênea convexa |
Natureza |
dissecação |
Caracteristica |
dissecação homogênea ou diferencial |
Forma |
topo convexo |
Densidade_Drenagem |
alta |
Aprofundamento_Incisoes |
fraco : > 50 a 100m |
Nivel_Altimetrico |
|
Legenda |
Serra da Bodoquena |
Area_Poligono_Km2 |
1.55 |
the_geom |
MULTIPOLYGON (((-56.96729223816305 -19.8924673236291, -56.96889613533847 -19.890651772047995, -56.96932513558302 -19.890022491422346, -56.97030549626774 -19.88888035725017, -56.97073514304879 -19.888308543960896, -56.971653995408154 -19.887165224376037, -56.97167360709263 -19.884579646870176, -56.97094969055643 -19.883770542939523, -56.97022427640888 -19.883421234037705, -56.96943582942074 -19.88335811584398, -56.968461095144896 -19.883809606737536, -56.96675406348781 -19.884659888351063, -56.96529323641306 -19.885281423068363, -56.96444580598504 -19.884930613928837, -56.96432942712398 -19.884240298119142, -56.963970942137685 -19.883547891345344, -56.96391571773227 -19.882743822985304, -56.963738166168845 -19.881995745982834, -56.96325863858508 -19.881302744763524, -56.96247363643469 -19.880779796649435, -56.9618068757671 -19.88060320383836, -56.96113694548672 -19.8806556316502, -56.960648336920165 -19.881111263664373, -56.96034040838585 -19.881913534045164, -56.95984644377096 -19.882829896566534, -56.959418052925535 -19.88334420178398, -56.95941177881359 -19.884147982129985, -56.95928383527314 -19.885066116664238, -56.95927819134366 -19.885755846280308, -56.95939141534017 -19.886847610444477, -56.95906436038026 -19.890120532500692, -56.959484958325525 -19.89069919049186, -56.95996421333362 -19.89162211031639, -56.96044439152672 -19.89237170293812, -56.960560143822136 -19.893176987243784, -56.96072762221311 -19.894902243886232, -56.96095789197719 -19.896742732883727, -56.96161342820737 -19.89846946049443, -56.96258228392872 -19.898765204686796, -56.96361446561575 -19.89871457297919, -56.96495748408702 -19.89786339877229, -56.96569415177631 -19.896660810924143, -56.96606515711132 -19.8957447298014, -56.96619152823831 -19.895113057374825, -56.96662274760981 -19.894254754068903, -56.967182207664614 -19.892591444434068, -56.96729223816305 -19.8924673236291))) |
gov
Trata-se de um conjunto de informações gráficas (pontos, linhas e polÃgonos) e alfanuméricas, georreferenciadas, interpretadasem escala 1:250.000, que retratam caracterÃsticas geomorfológicas da Folha XXX conforme metodologia contida no Manual Técnicode Geomorfologia (ftp://geoftp.ibge.gov.br/documentos/recursos_naturais/manuais_tecnicos/manual_tecnico_geomorfologia.pdf). São delineados e descritos polÃgonos de modelados de relevo contendo suanatureza genética, Unidade e Região Geomorfológica e o DomÃnio Morfoestrutural no qual estão inseridos. Também são representadas,por linhas e pontos, as principais formas de relevo encontradas no paÃs.A metodologia descrita no Manual Técnico de Geomorfologia é uma evolução dos procedimentos metodológicos adotados pelo projetoRADAMBRASIL no mapeamento geomorfológico do Brasil na escala de 1:1.000.000. O processo de elaboração dos mapas consistedas seguintes etapas: (1) estudo preliminar da área com a aquisição de bibliografia, documentos cartográficos e produtosde sensoreamento remoto, (2) elaboração de mapa geomorfológico preliminar com a análise da drenagem e delimitação de modeladose formas de relevo, apontando os locais de dúvida e de interesse para a terceira etapa, (3) atividade de campo, que tem comoobjetivo, além de solucionar dúvidas, o reconhecimento de caracterÃsticas do relevo com preenchimento de formulários de campoe registros fotográficos, (4) reinterpretação do mapeamento com base nas informações obtidas em campo, e (5) armazenamentodas informações gráficas e alfanuméricas em banco de dados para posterior consulta, tratamento,e/ou edição.
ver Fonte/+info (dt.atualização: 12/06/2018)
FID |
GeomorfologiaSE21.fid-6d9cbe3e_18e3b294723_66d2 |
Folha |
SE21 |
Legenda_Completa |
474Apf |
Nome_Dominio |
Depósitos Sedimentares Quaternários |
Nome_Regiao |
PlanÃcies e Pantanais Matogrossenses |
Identificacao_Unidade |
474 |
Nome_Unidade |
Pantanal do Miranda-Aquidauana |
Letra_Simbolo |
Apf |
Categoria |
PlanÃcie fluvial |
Natureza |
acumulação |
Caracteristica |
fluvial |
Forma |
planÃcie |
Densidade_Drenagem |
|
Aprofundamento_Incisoes |
|
Nivel_Altimetrico |
|
Legenda |
Pantanal do Miranda-Aquidauana |
Area_Poligono_Km2 |
48.173 |
the_geom |
MULTIPOLYGON (((-56.82814204362226 -19.774792443945806, -56.82571666001881 -19.774543332229165, -56.82425713231343 -19.774991636702403, -56.822553273363766 -19.77566758201922, -56.82154593140527 -19.775752496368945, -56.82044115231066 -19.77659695039971, -56.81960052337957 -19.777093266505588, -56.817390072372426 -19.7784347281405, -56.8167622295935 -19.778895816510772, -56.81609410956499 -19.77900535078087, -56.81528691058863 -19.779129658999203, -56.814289085050596 -19.77902951591463, -56.81244908384813 -19.778926513304317, -56.81113385606294 -19.77967146678649, -56.809766452377566 -19.780565938642944, -56.809078806591884 -19.781361552619398, -56.808287616664714 -19.781815181684046, -56.808081648948495 -19.78320240961623, -56.80798434584316 -19.783709679233404, -56.80749531787302 -19.78422331855225, -56.80676504156608 -19.784448334390014, -56.80488101073997 -19.784720078099532, -56.80324158973507 -19.784878191564754, -56.80135956600278 -19.784979312835215, -56.79790225410359 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